INTRODUCTION Water composes one of the five “spheres” in which environmental chemistry is discussed. This chapter introduces the environmental chemistry of water. Chapter 12 covers water pollution, and Chapter 13 discusses water treatment. THE PROPERTIES OF WATER, A UNIQUE SUBSTANCE Water has a number of unique properties that are essential to life and that determine its environmental chemical behavior. Many of these properties are due to water is polar molecular structure and its ability to form hydrogen bonds. The more important special characteristics of water are summarized in Table 11.1. in the text.
THE PROPERTIES OF WATER - Excellent solvent - Highest dielectric constant of any common liquid. - Higher surface tension than any other liquid. - Transparent to visible and longer-wavelength fraction of ultraviolet light. - Maximum density as liquid at 4 oC. - Higher heat of evaporation than any other material. - Higher latent heat of fusion than any other liquid except ammonia - Higher heat capacity than any other liquid except ammonia Water for Use: The water that humans use is primarily fresh surface water groundwater, Saline or brackish groundwater may also be utilized in some areas. Oceanic water(in arid region)
Efforts to conserve water: Since about 1980, water use in the U.S. has shown an encouraging trend with totalconsumption down by about 9% during a time in which population grew 16%, according to figures compiled by the U.S. Geological Survey. Industrial sector: Conservation and recycling have accounted for much of the decreased use in this sector. Irrigation water: replacing spray irrigators, lose large quantities of water to the action of wind and to evaporation, with irrigation systems that apply water directly to soil. Trickle (dripping) irrigation systems that apply just the amount of water needed directly to plant roots are especially efficient.
THE CHARACTERISTICS OF BODIES OF WATER The physical condition of a body of water strongly influences the chemical and biological processes that occur in water. Surface water: is found primarily in streams, lakes, and reservoirs. Wetlands: are productive flooded areas in which the water is shallow enough to enable growth of bottom-rooted plants. Estuaries: consisting of arms of the ocean into which streams flow. The mixing of fresh and salt water gives estuaries unique chemical and biological properties. Estuaries are the breeding grounds of much marine life, which makes their preservation very important. Water’s unique temperature-density relationship results in the formation of distinct layers within non flowing bodies of water, as shown in Figure
Thermal stratification: during the summer a surface layer (Epilimnion) is heated by solar radiation and, because of its lower density, floats upon the bottom layer, or (Hypolimnion). This phenomenon called thermal stratification, which means that When an appreciable temperature difference exists between the two layers, they do not mix, but behave independently and have very different chemical and biological properties
The epilimnion: which is exposed to light, may have a heavy growth of algae. As a result of exposure to the atmosphere and (during daylight hours) because of the photosynthetic activity of algae, the epilimnion contains relatively higher levels of dissolved oxygen and generally is “aerobic”. Because of the presence of O2 oxidized species predominate in the epilimnion. In the hypolimnion: consumption of O2 by bacterial action on biodegradable organic material may cause the water to become “anaerobic”. As a consequence, chemical species in a relatively reduced form tend to predominate in the hypolimnion. Oceans: the chemistry and biology of the oceans are unique because of the ocean’s high salt content, great depth, and other factors. The environmental problems of the oceans have increased greatly in recent years because of ocean dumping of pollutants, oil spills, and increased utilization of natural resources from the oceans.
AQUATIC CHEMISTRY This Figure summarizes important aspects of aquatic chemistry applied to environmental chemistry. As shown in this figure, a number of chemical phenomena occur in water. Many aquatic chemical processes are influenced by the action of algae and bacteria in water. For example, algal photosynthesis fixes inorganic carbon from HCO3- ion in the form of biomass (represented as CH2O) in a process that also produces carbonate ion, CO32-. Carbonate undergoes an acid-base reaction to produce OH- ion and raise the pH, or it reacts with Ca2+ ion to precipitate solid CaCO3.
Oxidation-reduction reactions in water: Most of the many oxidation-reduction reactions that occur in water are mediated (catalyzed) by bacteria. For example: In the oxygen-deficient (anaerobic) lower layers of a body of water bacteria convert inorganic nitrogen largely to ammonium ion, NH4+. Near the surface: where O2 is available bacteria convert inorganic nitrogen to nitrate ion, NO3-. Metals in water may be bound to organic chelating agents, such as pollutant nitrilotriacetic acid (NTA) or naturally occurring fulvic acids.
Gases are exchanged with the atmosphere, and various solutes are exchanged between water and sediments in bodies of water. Several important characteristics of unpolluted water should be noted. Some of these are: Gas solubility: Oxygen is the most important dissolved gas in water, since it is required to support aquatic life and maintain water quality. Water in equilibrium with air at 25 oC contains 8.3 (mg/L) of dissolved O2 . Water alkalinity: is defined as the ability of solutes in water to neutralize added strong acid. Water hardness: is due to the presence of calcium ion, Ca2+, and, to a lesser extent, magnesium ion, Mg2+.
ALKALINITY AND ACIDITY Alkalinity: isthe capacity of water to accept H+ ions (protons). Alkalinity is important in water treatment and in the chemistry and biology of natural waters. Frequently, the alkalinity of water must be known to calculate the quantities of chemicals to be added in treating the water. Highly alkaline water often has a high pH and generally contains elevated levels of dissolved solids. These characteristics may be detrimental for water to be used in boilers, food processing, and municipal water systems. Alkalinity serves as a pH buffer and reservoir for inorganic carbon, thus helping to determine the ability of water to support algal growth and other aquatic life. It is used by biologists as a measure of water fertility.
The basic species responsible for alkalinity in water are bicarbonate ion, carbonate ion, and hydroxide ion: HCO3- + H+ → CO2 + H2O CO32- + H+ → HCO3- OH- + H+ → H2O Other, usually minor, contributors to alkalinity are ammonia and the conjugate bases of phosphoric, silicic, boric, and organic acids.
It is important to distinguish between high basicity, manifested by an elevated pH, and high alkalinity, the capacity to accept H+. Whereas pH is an intensity factor, alkalinity is a capacity factor. As an example of a water-treatment process in which water alkalinity is important, consider the use of filter alum, Al2(SO4)3.18H2O as a coagulant. The hydrated aluminum ion is acidic, and, when it is added to water, it reacts with base to form gelatinous aluminum hydroxide, Al (H2O) 63+ + 3OH- → Al (OH) 3 (s) + 6H2O which settles and carries suspended matter with it. This reaction removes alkalinity from the water. Sometimes, the addition of more alkalinity is required to prevent the water from becoming too acidic.
In engineering terms, alkalinity frequently is expressed in units of mg/L of CaCO3, based upon the following acid-neutralizing reaction: CaCO3 + 2H+ → Ca2+ + CO2 + H 2O The equivalent weight of calcium carbonate is one-half its formula weight because only one-half of a CaCO3 molecule is required to neutralize one H+. Expressing alkalinity in terms of mg/L of CaCO3 can, however, lead to confusion, and equivalents/L is preferable notation for the chemist.
Acidity: as applied to natural water systems is the capacity of the water to neutralize OH- . Acidic water is not frequently encountered, except in cases of severe pollution. Acidity generally results from the presence of weak acids such as H2PO4-, CO2, H2S, proteins, fatty acids, and acidic metal ions, particularly Fe3+. Acidity is more difficult to determine than is alkalinity. One reason for the difficulty in determining acidity is that two of the major contributors are CO2 and H2S, both volatile solutes that are readily lost from the sample. The acquisition and preservation of representative samples of water to be analyzed for these gases is difficult. The term free mineral acid is applied to strong acids such as H2SO4 and HCl in water. Polluted acid mine water contains an appreciable concentration of free mineral acid.
Determination of total acidity by titration with base to the phenolphthalein (ph.ph.) endpoint (pH 8.2, where both strong and weak acids are neutralized), free mineral acid is determined by titration with base to the methyl orange (M.O.) endpoint (pH 4.3, where only strong acids are neutralized). The acidic character of some hydrated metal ions may contribute to acidity as shown by the following example: Al(H2O)63+ + H2O → Al(H2O)5OH2+ + H3O+ For simplicity, the above equation is expressed as Al(H2O)63+ → Al(H2O)5OH2+ + H+
Some industrial wastes, contain acidic metal ions and often some excess strong acid. For such wastes, the determination of acidity is important in calculating the amount of lime, or other chemicals, that must be added to neutralize the acid.
METAL IONS AND CALCIUM IN WATER Metal ions in water, commonly denoted Mn+, exist in numerous forms. Despite what the formula implies, a bare metal ion, Mg2+ for example, cannot exist as a separate entity in water. To secure the highest stability of their outer electron shells, metal ions in water are bonded, or coordinated, to water molecules in forms such as the hydrated metal cation M(H2O)xn+ , or other stronger bases (electron-donor partners) that might be present. Metal ions in aqueous solution seek to reach a state of maximum stability through chemical reactions including: 1- acid-base: Fe(H2O) 63+ → FeOH(H2O) 52+ + H+
2- precipitation, Fe(H2O)63+ → Fe(OH)3(s) + 3H2O + 3H+ 3- oxidation-reduction reactions Fe(H2O)62+ → Fe(OH)3(s) + 3H2O + e- + 3H+ Because of reactions such as these and the formation of dimeric species, such as Fe2(OH)24+, the concentration of simple hydrated Fe(H2O)63+ ion in water is vanishingly small; the same holds true for many other ionic species dissolved in water.